Petroleum Sources: Kerogen Types and Their Significance
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Sources of Petroleum
Petroleum originates from a small fraction of the organic matter deposited in sedimentary environments.
“Source Rock”
The typical “source rock” contains 99% mineral matter and 1% organic matter. The organic matter is composed of 90% kerogen and 10% bitumens.
This organic matter is usually a combination of marine- and terrestrially-derived organic matter (plant) and zooplankton (animal), which constitutes more than 95% of the life in the oceans.
Terrestrial organisms are mainly wind-blown spores and pollen, along with some woody debris from rivers and swamps.
All living matter is composed of four main constituents: lipids, proteins, carbohydrates, and lignins.
Kerogen Types
1. Type I Kerogen
This type of kerogen has a high... Continue reading "Petroleum Sources: Kerogen Types and Their Significance" »